Lattice defects in nonstoichiometric calcium hydroxylapatites. A

Lattice defects in nonstoichiometric calcium hydroxylapatites. A chemical approach. John L. Meyer, and Bruce O. Fowler. Inorg. Chem. , 1982, 21 (8), p...
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Inorg. Chem. 1982, 21, 3029-3035 may result that will produce two different iron sites. In view of the small difference of the two A,?? values, uiz., AEq' = 2.41 mm s-l and AEq"= 1.99 mm s-P at 115.1 K, and the identical temperature dependence of the quadrupole splitting, both iron(I1) atoms will have presumably the same ground state. In contrast to several related tran~itions,2'.~*~~ an orbital ground-state reversal may thus be ruled out for [Fe(bi),](C104)2. In the low-spin 'Al phase, the inequivalence of the

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two iron sites is not resolved due to the much smaller value of AEq('A,), which is insensitive to lattice distortions.

Acknowledgment. The authors appreciate financial support by the Stiftung Volkswagenwerk and the Fonds der Chemischen Industrie. Thanks are also due to Dr. V. McKee for her assistance in the preparation of the samples. Registry No. [Fe(bi),] (C10J2, 755 16-37-9.

Contribution from the Laboratory of Biological Structure, National Institute of Dental Research, National Institutes of Health, Bethesda, Maryland 20205

Lattice Defects in Nonstoichiometric Calcium Hydroxylapatites. A Chemical Approach JOHN L. MEYER' and BRUCE 0. FOWLER

Received September 25, 1981 A number of defect hydroxylapatites were prepared with Ca/P molar ratios varying from 1.40 to 1.62. These samples were analyzed for their hydroxide contents by a titration method after chemically determining their calcium, phosphate, acid phosphate, and carbonate contents. The results were compared with various general compositional formulas previously used to describe the structure and composition of the defect hydroxylapatites. Hydroxide contents between 0 and 1.13 per theoretical unit cell of hydroxylapatite, Ca10(P04)6(OH)2, were obtained depending upon experimental conditions. The general compositional formula that best represented the experimental data was C a I ~ ~ - Y ( H P 0 , ) ~ ~ 4 ) 6 0 H ) 2 -which X-2Y, describes two types of calcium vacancies in the defect lattice. The first, or X type, is coupled to the loss of a hydroxide and the addition of a hydrogen ion to the lattice and seem to be dependent upon the conditions of preparation of the precipitates. The second calcium vacancy (Y type) is electrically compensated by two vacant hydroxide positions and seems to be insensitive to solution environment with an average of about 0.5 calcium vacancy per unit cell. Other models that assume only X-type vacancies or that require one or more hydroxides for lattice stability seem to be in error.

Introduction Hydroxylapatite (HA, Calo(P04)6(0H)2)serves as a model structural component for all the calcium-containing apatites of biological interest.' The inorganic apatitic materials present in biological hard tissue, with the possible exception of dental enamel, have carbonate-corrected calcium/phosphate molar ratios less than the theoretical 1.67, and a number of theories have been advanced to explain this discrepancy. One suggestion was that the defect hydroxylapatites (DHA) or nonstoichiometric hydroxylapatites contained the theoretical amount of hydroxide and that the low calcium phosphate ratios were due entirely to calcium ion defects with electroneutrality being maintained by the presence of two protons in the lattice for each missing ~ a l c i u m . ~ -This ~ concept results in the general formula I in Table I for the DHAs. Winand et later proposed the alternative formula 11, which suggests that both calcium and hydroxide defects can occur. Hydrogen ion enters the lattice in this formulation also but must necessarily be coupled with the removal of a calcium and a hydroxide ion from the lattice. Kuhl and Nebergall' proposed the more general formula 111, which maintains electroneutrality by a combination of (a) a one-proton addition for each calcium and hydroxide defect and (b) the absence of two hydroxides per calcium ion defect. Kuhl and Nebergall' also allowed for the uptake of carbonate by the apatite lattice by suggesting formula IV, which substitutes C03*-for HPO?-. Berry,8 using McLean, F. C.; Urist, M. R.'Bone"; The University of Chicago Press: Chicago, 1961;p 148. Posner, A. S.;Perloff, A. J. Res. Natl. Bur. Stand. ( U S . )1957,58,279. Posner, A. S.; Stutman, J. M.; Lippinwtt, E. R. Nature (London) 1960, ~.

Table I. General Compositional Formulas for Defect Calcium Hydroxylapatites ~

ref

Cal,~(~~~,)2X~~~,)6_2X(~~), o < x 6 -2 C~,,-~(HPO,)X(PO,)~-X(OH)~-X 0 < XG 2 C~I,-~-~(HPO,)~(PO,)~-~o < x < 2,

2-4 5,6 7

Iv

(OH) 2-X-2 y Cai 0-x- Y(HPO, , c o O)x(po4)6-x(OH)?-x-zy

7

V

Ca,,_X(HPO,)X(PO,),-X(OH),-x Ca/P B 1.5,

8, 10

VI

Ca,_x(HPO,),+,x(PO,)s-lx(OH) Ca/P G 1.5,

9, 11

1

11 111

formula

~ _ _ _ _

remarks

no.

Y < 1-XI2

o < x < 2,

Y < 1- x / 2

o < x